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Museum of Appalachia. The Museum of Appalachia, located in Norris, Tennessee, 20 miles (32 km) north of Knoxville, is a living history museum that interprets the pioneer and early 20th-century period of the Southern Appalachian region of the United States. Recently named an Affiliate of the Smithsonian Institution, the museum is a collection of ...
The Appalachian Mountains formed through a series of mountain-building events over the last 1.2 billion years: [4] [5] The Grenville orogeny began 1250 million years ago (Ma) and lasted for 270 million years. The Taconic orogeny began 450 Ma and lasted for 10 million years. The Acadian orogeny began 375 Ma and lasted 50 million years.
The Appalachian Mountains, [b] often called the Appalachians, are a mountain range in eastern to northeastern North America. The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used is one followed by the United States Geological Survey and the ...
A timber cutter's mountain log cabin at the Museum of Folk Architecture and Life in Pyrohiv, Ukraine. A log cabin is a small log house, especially a minimally finished or less architecturally sophisticated structure. Log cabins have an ancient history in Europe, and in America are often associated with first-generation home building by settlers.
Appalachian Plateau. Coordinates: 40°N 78°W. Appalachian Plateau province of Appalachian Highlands division. The Appalachian Plateau is a series of rugged dissected plateaus located on the western side of the Appalachian Mountains. The Appalachian Mountains are a range that run from Nova Scotia in Canada to Alabama in the United States.
Single-pen architecture and double-pen architecture are architectural styles for design of log, and sometimes stone or brick pioneer houses found in the United States. A single pen is just one unit: a rectangle of four walls of a log cabin. In double pen architecture, two log pens are built and those are joined by a roof over a breezeway in ...
The Alleghanian orogeny or Appalachian orogeny is one of the geological mountain-forming events that formed the Appalachian Mountains and Allegheny Mountains. The term and spelling Alleghany orogeny was originally proposed by H.P. Woodward in 1957. The Alleghanian orogeny occurred approximately 325 million to 260 million years ago [1] over at ...
The following is a comprehensive list of historical structures located within and maintained by the Great Smoky Mountains National Park. Structures at Cades Cove, Roaring Fork, the Noah Ogle Place, and Elkmont are part of U.S. Registered Historic Districts. Nine individual structures in the park are listed on the National Register of Historic ...
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